The Chemically Altered Basaltic Northern Plains of Mars: TES, OMEGA, and GRS Integrated Data Sets and Conclusions

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Scientific paper

TES, OMEGA, and GRS data sets lead to the following conclusions: 1) the
northern plains are basaltic; 2) the basalt is chemically altered; and
3) the alteration likely resulted from surface interactions with
volatiles (snow) deposited during phases of high obliquity.

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